Two-Tiered Transition of the North Atlantic Surface Hydrology during the Past 1.6 Ma: Multiproxy Evidence from Planktic Foraminifera-Reference-Cited by-同舟云学术

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Two-Tiered Transition of the North Atlantic Surface Hydrology during the Past 1.6 Ma: Multiproxy Evidence from Planktic Foraminifera

Published:2021-10-01 Issue:4 Volume:25 Page:
ISSN:1342-8144
Container-title:Paleontological Research
language:
Short-container-title:Paleontological Research

Author:

Yamasaki Makoto¹,Shimada Chieko²,Ikehara Minoru³,Schiebel Ralf⁴

Affiliation:

1. Department of Earth Resource Science, Graduate school of International Resource Sciences, Akita University, Tegata-Gakuenmachi 1-1, Akitashi, Akita 010-8502, Japan (e-mail: )

2. Department of Geology and Paleontology, National Museum of Nature and Science, Amakubo 4-1-1, Tsukuba-shi, Ibaraki 305-0005, Japan

3. Center for Advanced Marine Core Research (CMCR), Kochi University, Monobe-Otsu 200, Nankoku-shi, Kochi 783-8502, Japan

4. Climate Geochemistry, Max Planck Institute for Chemistry, Hahn-Meitner-Weg 1, 55128 Mainz, Germany

Publisher

The Paleontological Society of Japan

Subject

Paleontology,Ecology, Evolution, Behavior and Systematics

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